Man and the Glacial PeriodWright, G. Frederick (George Frederick)
History
Man and the Glacial Period
Wright, G. Frederick (George Frederick)
Glacial epoch; Prehistoric peoples
On the part of many the theory here provisionally adopted will be
regarded with disfavour by reason of a disinclination to supposing
any great recent changes of level in the continental areas. So firmly
established do the continents appear to be, that it seems like invoking
an inordinate display of power to have them exalted for the sake of
producing a Glacial period. Due reflection, however, will make it
evident that within certain limits the continents are exceedingly
unstable, and that they have displayed this instability to as great an
extent in recent geological times as they have done in any previous
geological periods. When one reflects, also, upon the size of the earth,
a continental elevation of 3,000 or 4,000 feet upon a globe whose
diameter is more than 40,000,000 feet is an insignificant trifle. On a
globe one foot in diameter it would be represented by a protuberance of
barely one thousandth of an inch. A corresponding wrinkle upon a large
apple would require a magnifying-glass for its detection. Moreover, the
activity of existing volcanoes, the immense outflows of lava which have
taken place in the later geological periods, together with the uniform
increase of heat as we penetrate to deeper strata in the crust of the
earth--all point to a condition of the earth's interior that would
make the elevations of land which we have invoked for the production
of the Glacial period easily credible. Physicists do not, indeed, now
hold to the entire fluidity of the earth's interior, but rather to a
solid centre, where gravity overcomes the expansive power of heat, and
maintains solidity even when the heat is intense. But between the cooling
crust of the earth's exterior and a central solid core there is now
believed to be a film where the influences of heat and of the pressure
of gravity are approximately balanced, and the space is occupied by a
half-melted or viscous magma, capable of yielding to a slow pressure, and
of moving in response to it from one portion of the enclosed space to
another where the pressure is for any cause relieved.
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